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    五台群是新太古代还是古元古代?同位素年代学研究评述

    赵飞凡 陈衍景

    赵飞凡, 陈衍景, 2021. 五台群是新太古代还是古元古代?同位素年代学研究评述. 地球科学, 46(1): 1-12. doi: 10.3799/dqkx.2020.019
    引用本文: 赵飞凡, 陈衍景, 2021. 五台群是新太古代还是古元古代?同位素年代学研究评述. 地球科学, 46(1): 1-12. doi: 10.3799/dqkx.2020.019
    Zhao Feifan, Chen Yanjing, 2021. Is the Wutai Group of Neoarchean or Paleoproterozoic? A Review of Isotope Chronological Studies. Earth Science, 46(1): 1-12. doi: 10.3799/dqkx.2020.019
    Citation: Zhao Feifan, Chen Yanjing, 2021. Is the Wutai Group of Neoarchean or Paleoproterozoic? A Review of Isotope Chronological Studies. Earth Science, 46(1): 1-12. doi: 10.3799/dqkx.2020.019

    五台群是新太古代还是古元古代?同位素年代学研究评述

    doi: 10.3799/dqkx.2020.019
    基金项目: 

    国家自然科学基金项目 U1906207

    国家自然科学基金项目 41890833

    国家重点基础研究发展计划(“973”计划) 2012CB416602

    详细信息
      作者简介:

      赵飞凡(1995-), 男, 硕士研究生, 矿物学、岩石学、矿床学专业.ORCID:0000-0001-9803-5663.E-mail:839963725@qq.com

      通讯作者:

      陈衍景, ORCID:0000-0001-9211-4993.E-mail:yjchen@pku.edu.cn

    • 中图分类号: P597

    Is the Wutai Group of Neoarchean or Paleoproterozoic? A Review of Isotope Chronological Studies

    • 摘要: 五台群长期被多数学者作为新太古代地层,自下而上分为石咀亚群、台怀亚群和高凡亚群,但同位素年代学研究给出了一些古元古代年龄,致使五台群形成时代及地层划分对比方案悬而未决.全面收集了五台群已有同位素年龄数据,仅锆石U-Pb谐和年龄数据就有800多组.数据显示,高凡亚群包括洪寺组和羊蹄沟组,沉积时间不早于2 331±38 Ma,属于古元古代层侵纪.台怀亚群包括柏枝岩组和鸿门岩组,鸿门岩组结晶年龄约为2 435±64 Ma,柏枝岩组沉积年龄为2 435±64~2 468±61 Ma,故台怀亚群形成于2 435±64~2 468±61 Ma,属古元古代成铁纪.石咀亚群自下而上分为板峪口组、金岗库组、庄旺组、文溪组,其中,文溪组和板峪口组缺乏同位素年龄数据,庄旺组形成于2 468±61 Ma,金岗库组形成于2 468±61~2 494±29 Ma,属于古元古界底部.结合五台花岗绿岩地体之花岗岩类的年龄(>2 520 Ma),认为五台群之下存在花岗质岩石基底.五台地区锆石年龄还表现出了~2.7 Ga和~2.5 Ga的年龄峰值,指示新太古代发生了两次地壳快速生长.五台地区2.52~2.56 Ga的花岗质岩石显示岛弧特征,表明板块俯冲作用在新太古代地壳生长中扮演了重要角色.

       

    • 图  1  五台地区地质图

      白瑾(1986)修改

      Fig.  1.  Simplified geological map of the Wutaishan area

      图  2  五台群岩性地层柱状图

      改编自白瑾(1986)

      Fig.  2.  Stratigraphic units of the Wutai Group

      图  3  高凡亚群样品及其侵入岩的锆石207Pb/206Pb年龄频数直方图

      数据引自Wilde et al.(2004)Liu et al.(2016a)Peng et al.(2017)

      Fig.  3.  Zircon 207Pb/206Pb age histogram of the Gaofan Subgroup and its intrusive rocks

      图  4  鸿门岩组样品的207Pb/206Pb锆石年龄频数直方图

      数据引自Sun et al.(2019)Wilde et al.(2004)

      Fig.  4.  Zircon 207Pb/206Pb age histogram of the Hongmenyan Formation

      图  5  柏枝岩组样品锆石207Pb/206Pb年龄直方图

      数据引自Wilde et al.(2004)Liu et al.(2016a, 2016b)

      Fig.  5.  Zircon 207Pb/206Pb age histogram of the Baizhiyan Formation

      图  6  庄旺组样品锆石207Pb/206Pb年龄直方图

      数据引自Wilde et al.(2004)Liu et al.(2016a)

      Fig.  6.  Zircon 207Pb/206Pb age histogram of the Zhuangwang Formation

      图  7  金岗库组样品及其侵入岩锆石207Pb/206Pb年龄直方图

      数据来源:Wang et al.(2014)陈雪等(2015)Liu et al.(2016a)赵娜等(2019)

      Fig.  7.  Zircon 207Pb/206Pb age histogram of the Jin'gangku Formation and its intrusive rocks

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